Earth and Planetary Science Letters

Papers
(The TQCC of Earth and Planetary Science Letters is 13. The table below lists those papers that are above that threshold based on CrossRef citation counts [max. 250 papers]. The publications cover those that have been published in the past four years, i.e., from 2020-05-01 to 2024-05-01.)
ArticleCitations
Sedimentary host phases of mercury (Hg) and implications for use of Hg as a volcanic proxy125
China's Chang'e-5 landing site: Geology, stratigraphy, and provenance of materials100
The early Eocene rise of the Gonjo Basin, SE Tibet: From low desert to high forest92
Young lunar mare basalts in the Chang'e-5 sample return region, northern Oceanus Procellarum89
Qaidam Basin leaf fossils show northeastern Tibet was high, wet and cool in the early Oligocene80
Gondwana's interlinked peripheral orogens71
Paired metamorphism in the Neoarchean: A record of accretionary-to-collisional orogenesis in the North China Craton70
Potassium isotope fractionation during chemical weathering of basalts67
First evidence of eclogites overprinted by ultrahigh temperature metamorphism in Everest East, Himalaya: Implications for collisional tectonics on early Earth63
Rock strength and structural controls on fluvial erodibility: Implications for drainage divide mobility in a collisional mountain belt60
Mantle influx compensates crustal thinning beneath the Cathaysia Block, South China: Evidence from SINOPROBE reflection profiling60
IMS observations of infrasound and acoustic-gravity waves produced by the January 2022 volcanic eruption of Hunga, Tonga: A global analysis60
Crustal-scale wedge tectonics at the narrow boundary between the Tibetan Plateau and Ordos block59
Qinghai-Tibet Plateau wetting reduces permafrost thermal responses to climate warming57
A Neoproterozoic low-δ18O m55
Late Pliocene onset of the Cona rift, eastern Himalaya, confirms eastward propagation of extension in Himalayan-Tibetan orogen52
Assessing seasonal and interannual water storage variations in Taiwan using geodetic and hydrological data52
Early evolution of the solar accretion disk inferred from Cr-Ti-O isotopes in individual chondrules50
Low-temperature oceanic crust alteration and the isotopic budgets of potassium and magnesium in seawater49
Peel-back controlled lithospheric convergence explains the secular transitions in Archean metamorphism and magmatism49
Enhanced chemical weathering triggered an expansion of euxinic seawater in the aftermath of the Sturtian glaciation48
TTG generation by fluid-fluxed crustal melting: Direct evidence from the Proterozoic Georgetown Inlier, NE Australia47
Slab dehydration in warm subduction zones at depths of episodic slip and tremor46
A high-resolution Middle to Late Permian paleotemperature curve reconstructed using oxygen isotopes of well-preserved brachiopod shells46
Ice loss in the Northeastern Tibetan Plateau permafrost as seen by 16 yr of ESA SAR missions45
Evaluating a primary carbonate pathway for manganese enrichments in reducing environments44
Detrital zircon evidence for change in geodynamic regime of continental crust formation 3.7–3.6 billion years ago44
Redox controls during magma ocean degassing43
Dilatancy-induced fluid pressure drop during dynamic rupture: Direct experimental evidence and consequences for earthquake dynamics43
Europium and barium enrichments in compositionally zoned felsic tuffs: A smoking gun for the origin of chemical and physical gradients by cumulate melting43
Geophysical and cosmochemical evidence for a volatile-rich Mars42
Chemical evolution of the continental crust from a data-driven inversion of terrigenous sediment compositions42
Explosivity of basaltic lava fountains is controlled by magma rheology, ascent rate and outgassing42
A catalogue of impact craters larger than 200 m and surface age analysis in the Chang'e-5 landing area42
Origin and evolution of fault-controlled hydrothermal dolomitization fronts: A new insight41
Expanse of Greater India in the late Cretaceous41
Origin of volatile element depletion among carbonaceous chondrites41
The tungsten-182 record of kimberlites above the African superplume: Exploring links to the core-mantle boundary40
U-Pb zircon age constraints on the earliest eruptions of the Deccan Large Igneous Province, Malwa Plateau, India40
Generation of Eoarchean continental crust from altered mafic rocks derived from a chondritic mantle: The ∼3.72 Ga Aktash gneisses, Tarim Craton (NW China)40
A plume-modified lithospheric barrier to the southeastward flow of partially molten Tibetan crust inferred from magnetotelluric data39
A disordered kinetic model for clumped isotope bond reordering in carbonates39
Global and local drivers of the Ediacaran Shuram carbon isotope excursion39
The 2018-ongoing Mayotte submarine eruption: Magma migration imaged by petrological monitoring39
The micrometeorite flux at Dome C (Antarctica), monitoring the accretion of extraterrestrial dust on Earth39
Interannual flow dynamics driven by frontal retreat of a lake-terminating glacier in the Chinese Central Himalaya38
An evaluation of the C/N ratio of the mantle from natural CO2-rich gas analysis: Geochemical and cosmochemical implications38
Holocene variability of East Asian summer monsoon as viewed from the speleothem δ38
Short duration of Early Permian Qiangtang-Panjal large igneous province: Implications for origin of the Neo-Tethys Ocean38
Active crustal deformation and rotations in the southwestern Balkans from continuous GPS measurements38
Astrochronology of the Ediacaran Shuram carbon isotope excursion, Oman37
Spatio-temporal foreshock evolution of the 2019 M 6.4 and M 7.1 Ridgecrest, California earthquakes36
A dynamic lithosphere–asthenosphere boundary near the equatorial Mid-Atlantic Ridge36
Long-lived (ca. 22–24 Myr) partial melts in the eastern Himalaya: Petrochronologic constraints and tectonic implications36
Northwest Pacific-Izanagi plate tectonics since Cretaceous times from western Pacific mantle structure34
Petrochronological close-up on the thermal structure of a paleo-subduction zone (W. Alps)34
The tilted Iceland Plume and its effect on the North Atlantic evolution and magmatism34
Deciphering the evolution and forcing mechanisms of glaciation over the Himalayan-Tibetan orogen during the past 20,000 years34
Towards balancing the oceanic Ni budget34
Characteristic landslide distributions: An investigation of landscape controls on landslide size34
The stabilizing effect of high pore-fluid pressure along subduction megathrust faults: Evidence from friction experiments on accretionary sediments from the Nankai Trough33
Was climatic cooling during the earliest Carboniferous driven by expansion of seed plants?33
A coupled carbon-silicon cycle model over Earth history: Reverse weathering as a possible explanation of a warm mid-Proterozoic climate33
Subsolar Al/Si and Mg/Si ratios of non-carbonaceous chondrites reveal planetesimal formation during early condensation in the protoplanetary disk33
Geodetic imaging of shallow creep along the Xianshuihe fault and its frictional properties32
Temperature changes across the Paleocene-Eocene Thermal Maximum – a new high-resolution TEX86 temperature record from the Eastern North Sea Basin32
Temperature signals of ice core and speleothem isotopic records from Asian monsoon region as indicated by precipitation δ18O32
Controls on the abundance, provenance and age of organic carbon buried in continental margin sediments32
The effect of wind speed averaging time on the calculation of sand drift potential: New scaling laws32
Controls on the magmatic fraction of extension at mid-ocean ridges32
Pervasive sources of isotopically light zinc in the North Atlantic Ocean32
Geochronologic constraints on deformation and metasomatism along an exhumed mylonitic shear zone using apatite U-Pb, geochemistry, and microtextural analysis32
Magnesium isotopic fractionation during basalt differentiation as recorded by evolved magmas31
A 3800 yr paleoseismic record (Lake Hazar sediments, eastern Turkey): Implications for the East Anatolian Fault seismic cycle31
Frontal ablation and mass loss of the Patagonian icefields31
Global zircon analysis records a gradual rise of continental crust throughout the Neoarchean31
Strong shear softening induced by superionic hydrogen in Earth's inner core31
Atmospheric river changes shaped mid-latitude hydroclimate since the mid-Holocene30
Exploring laser ablation U–Pb dating of regional metamorphic garnet – The Straits Schist, Connecticut, USA30
Simulation of early Eocene water isotopes using an Earth system model and its implication for past climate reconstruction30
Pulsed oxygenation events drove progressive oxygenation of the early Mesoproterozoic ocean30
Origin of a global carbonate layer deposited in the aftermath of the Cretaceous-Paleogene boundary impact30
Evidence for crustal removal, tectonic erosion and flare-ups from the Japanese evolving forearc sediment provenance30
Climatic fluctuations modeled for carbon and sulfur emissions from end-Triassic volcanism30
New early oligocene zircon U-Pb dates for the ‘Miocene’ Wenshan Basin, Yunnan, China: Biodiversity and paleoenvironment29
Was the Pamir salient built along a Late Paleozoic embayment on the southern Asian margin?29
Expanded lacustrine sedimentation in the Qaidam Basin on the northern Tibetan Plateau: Manifestation of climatic wetting during the Oligocene icehouse29
Deformation-enhanced recrystallization of titanite drives decoupling between U-Pb and trace elements29
The evolution and distribution of recycled oceanic crust in the Earth's mantle: Insight from geodynamic models29
Slab-controlled elemental–isotopic enrichments during subduction initiation magmatism and variations in forearc chemostratigraphy29
Sediment and ocean crust both melt at subduction zones29
The triple oxygen isotope composition of Precambrian chert29
Post-depositional REE mobility in a Paleoarchean banded iron formation revealed by La-Ce geochronology: A cautionary tale for signals of ancient oxygenation29
Towards understanding the origin of massive dolostones29
Resistivity saturation of hcp Fe-Si alloys in an internally heated diamond anvil cell: A key to assessing the Earth's core conductivity28
Highly dynamic marine redox state through the Cambrian explosion highlighted by authigenic δ238U records28
The 22 July 2020 M 7.8 Shumagin seismic gap earthquake: Partial rupture of a weakly coupled megathrust28
Ti-in-quartz thermobarometry and TiO2 solubility in rhyolitic melts: New experiments and parametrization28
Climatic patterns over the European Alps during the LGM derived from inversion of the paleo-ice extent28
Partitioning riverine sulfate sources using oxygen and sulfur isotopes: Implications for carbon budgets of large rivers28
Scaling laws for the geometry of an impact-induced magma ocean27
Nucleosynthetic Pt isotope anomalies and the Hf-W chronology of core formation in inner and outer solar system planetesimals27
Large isotopic variability at the micron-scale in ‘Shuram’ excursion carbonates from South Australia27
Origin of hydrogen isotopic variations in chondritic water and organics27
Plate tectonics and mantle controls on plume dynamics27
Understanding ancient tectonic settings through detrital zircon analysis27
Orbitally-paced climate change in the early Cambrian and its implications for the history of the Solar System27
Astronomically forced climate change in the late Cambrian27
Unravelling Middle to Late Jurassic palaeoceanographic and palaeoclimatic signals in the Hebrides Basin using belemnite clumped isotope thermometry27
An extended period of extremely weak geomagnetic field suggested by palaeointensities from the Ediacaran Grenville dykes (SE Canada)27
Thermobarometry of CO2-rich, silica-undersaturated melts constrains cratonic lithosphere thinning through time in areas of kimberlitic magmatism27
Chondritic mercury isotopic composition of Earth and evidence for evaporative equilibrium degassing during the formation of eucrites27
Hotspots and mantle plumes revisited: Towards reconciling the mantle heat transfer discrepancy27
Co-seismic rupture of the 2021, M 7.4 Maduo earthquake (northern Tibet): Short-cutting of the Kunlun fault big bend26
Photochemical modelling of atmospheric oxygen levels confirms two stable states26
The young Sun's XUV-activity as a constraint for lower CO2-limits in the Earth's Archean atmosphere26
Hypocentral dependent shallow slip distribution and rupture extents along a strike-slip fault26
Can volcanism build hydrogen-rich early atmospheres?26
Geomorphologic exploration targets at the Zhurong landing site in the southern Utopia Planitia of Mars26
Mantle source characteristics and magmatic processes during the 2021 La Palma eruption26
Petrogenetic processes at the tipping point of plate tectonics: Hf-O isotope ternary modelling of Earth's last TTG to sanukitoid transition26
Strain localization and fluid-assisted deformation in apatite and its influence on trace elements and U–Pb systematics26
Detrital rutile ages can deduce the tectonic setting of sedimentary basins26
The role of inherited crustal and lithospheric architecture during the evolution of the Red Sea: Insights from three dimensional analogue experiments25
Crustal tilting and differential exhumation of Gangdese Batholith in southern Tibet revealed by bedrock pressures25
New cosmogenic nuclide burial-dating model indicates onset of major glaciations in the Alps during Middle Pleistocene Transition25
Fluid mixing as primary trigger for cassiterite deposition: Evidence from in situ δ18O-δ11B analysis of tourmaline from the world-class San Rafael tin (-copper) deposit, Peru25
Limited iodate reduction in shipboard seawater incubations from the Eastern Tropical North Pacific oxygen deficient zone25
Dislocation interactions during low-temperature plasticity of olivine and their impact on the evolution of lithospheric strength24
Deep learning for laboratory earthquake prediction and autoregressive forecasting of fault zone stress24
Three North African dust source areas and their geochemical fingerprint24
Transport properties of Fe-Ni-Si alloys at Earth's core conditions: Insight into the viability of thermal and compositional convection24
Controls on the cadmium isotope composition of modern marine sediments24
Preconditioning by sediment accumulation can produce powerful turbidity currents without major external triggers24
Timescales of subduction initiation and evolution of subduction thermal regimes24
Flotation mechanism of sulphide melt on vapour bubbles in partially molten magmatic systems24
Subcretionary tectonics: Linking variability in the expression of subduction along the Cascadia forearc24
Quantitative estimates of Holocene glacier meltwater variations on the Western Tibetan Plateau24
Westerly jet stream controlled climate change mode since the Last Glacial Maximum in the northern Qinghai-Tibet Plateau24
Assessing the presence of volatile-bearing mineral phases in the cratonic mantle as a possible cause of mid-lithospheric discontinuities24
On the petrogenesis of lunar troctolites: New insights into cumulate mantle overturn & mantle exposures in impact basins24
Warm and oxidizing slabs limit ingassing efficiency of nitrogen to the mantle24
Evidence for a regional warm bias in the Early Cretaceous TEX86 record24
The fate of fluvially-deposited organic carbon during transient floodplain storage24
Chromium isotope systematics and the diagenesis of marine carbonates24
Evidence for methane isotopic bond re-ordering in gas reservoirs sourcing cold seeps from the Sea of Marmara24
Cosmogenic 10Be production records reveal dynamics of geomagnetic dipole moment (GDM) over the Laschamp excursion (20–60 ka)24
Using stable isotopes to distinguish atmospheric nitrate production and its contribution to the surface ocean across hemispheres23
Zinc- and cadmium-isotope evidence for redox-driven perturbations to global micronutrient cycles during Oceanic Anoxic Event 2 (Late Cretaceous)23
The 2019 Ridgecrest, California earthquake sequence: Evolution of seismic and aseismic slip on an orthogonal fault system23
Isotopic fingerprinting of biogeochemical processes and iron sources in the iron-limited surface Southern Ocean23
The deep Shumagin gap filled: Kinematic rupture model and slip budget analysis of the 2020 Mw 7.8 Simeonof earthquake constrained by GNSS, global seismic waveforms, and floating InSAR23
The 2010 Haiti earthquake revisited: An acoustic intensity map from remote atmospheric infrasound observations23
Multicomponent diffusion of F, Cl and OH in apatite with application to magma ascent rates23
Predicting the proximity to macroscopic failure using local strain populations from dynamic in situ X-ray tomography triaxial compression experiments on rocks23
Appraisal of alkenone- and archaeal ether-based salinity indicators in mid-latitude Asian lakes23
Copper-mineralised porphyries sample the evolution of a large-volume silicic magma reservoir from rapid assembly to solidification23
Seismic and geodetic progression of the 2018 summit caldera collapse of Kīlauea volcano23
Black Sea paleosalinity evolution since the last deglaciation reconstructed from alkenone-inferred Isochrysidales diversity23
Long-term evolution of a plume-induced subduction in the Neotethys realm23
Polarity-reversal subduction zone initiation triggered by buoyant plateau obstruction23
Periodic oceanic euxinia and terrestrial fluxes linked to astronomical forcing during the Late Devonian Frasnian–Famennian mass extinction22
Cryogenian interglacial greenhouse driven by enhanced volcanism: Evidence from mercury records22
Kinematics of the ∼1000 km Haiyuan fault system in northeastern Tibet from high-resolution Sentinel-1 InSAR velocities: Fault architecture, slip rates, and partitioning22
Role of sulfate in the transport and enrichment of REE in hydrothermal systems22
On Archean craton growth and stabilisation: Insights from lithospheric resistivity structure of the Superior Province22
Rock abundance and evolution of the shallow stratum on Chang'e-4 landing site unveiled by lunar penetrating radar data22
Event-dominated transport, provenance, and burial of organic carbon in the Japan Trench22
Hydrothermal alteration associated with the Chicxulub impact crater upper peak-ring breccias22
Seismic hazard of the western Makran subduction zone: Insight from mechanical modelling and inferred frictional properties22
Coexisting diverse P–T–t paths during Neoarchean Sagduction: Insights from numerical modeling and applications to the eastern North China Craton22
Competition between preslip and deviatoric stress modulates precursors for laboratory earthquakes22
Molybdenum isotope systematics of lavas from the East Pacific Rise: Constraints on the source of enriched mid-ocean ridge basalt22
Disparities in oxygen isotopes of detrital and igneous zircon identify erosional bias in crustal rock record22
Southeastern margin of the Tibetan Plateau stopped expanding in the late Miocene22
Subduction initiation and the rise of the Shillong Plateau22
The phases of the Moon: Modelling crystallisation of the lunar magma ocean through equilibrium thermodynamics22
Pervasive low-velocity layer atop the 410-km discontinuity beneath the northwest Pacific subduction zone: Implications for rheology and geodynamics22
The role of incremental magma chamber growth on ore formation in porphyry copper systems22
Mercury isotope evidence for regional volcanism during the Frasnian-Famennian transition22
Thick, strong sediment subduction along south-central Chile and its role in great earthquakes22
A possible high-temperature origin of the Moon and its geochemical consequences22
The evolution of lithium isotope signatures in fluids draining actively weathering hillslopes22
Assessing the potential capability of reconstructing glacial Atlantic water masses and AMOC using multiple proxies in CESM22
Thermal conductivity of Fe-bearing post-perovskite in the Earth's lowermost mantle22
Reappraisal of purported ca. 3.7 Ga stromatolites from the Isua Supracrustal Belt (West Greenland) from detailed chemical and structural analysis22
Combination of Δ47 and U-Pb dating in tectonic calcite veins unravel the last pulses related to the Pyrenean Shortening (Spain)22
Into the deep and beyond: Carbon and nitrogen subduction recycling in secondary peridotites22
Enhanced water loss from the martian atmosphere during a regional-scale dust storm and implications for long-term water loss22
Layered crustal azimuthal anisotropy beneath the northeastern Tibetan Plateau revealed by Rayleigh-wave Eikonal tomography22
Glacial pumping of a magma-charged lithosphere: A model for glaciovolcanic causality in magmatic arcs22
Reversible scavenging traps hydrothermal iron in the deep ocean22
Calcium isotope constraints on OIB and MORB petrogenesis: The importance of melt mixing22
Metal-silicate mixing by large Earth-forming impacts22
Lower-altitude of the Himalayas before the mid-Pliocene as constrained by hydrological and thermal conditions22
Reconstruction of the 2018 tsunamigenic flank collapse and eruptive activity at Anak Krakatau based on eyewitness reports, seismo-acoustic and satellite observations22
Centimeter-resolution topographic modeling and fine-scale analysis of craters and rocks at the Chang'E-4 landing site22
Linking surface deformation to thermal and mechanical magma chamber processes21
Fault roughness controls sliding instability21
Mineral inclusions are not immutable: Evidence of post-entrapment thermally-induced shape change of quartz in garnet21
Evidence for crustal seismic anisotropy at the InSight lander site21
The temporal distribution of Earth's supermountains and their potential link to the rise of atmospheric oxygen and biological evolution21
Aquifer deformation and active faulting in Salt Lake Valley, Utah, USA21
Tsunami earthquakes: Vertical pop-up expulsion at the forefront of subduction megathrust21
Indian continental lithosphere and related volcanism beneath Myanmar: Constraints from local earthquake tomography21
The Ca and Mg isotope record of the Cryogenian Trezona carbon isotope excursion21
Controls on boron isotopes in a cold-water coral and the cost of resilience to ocean acidification21
Evaluation of shallow-water carbonates as a seawater zinc isotope archive21
Evolution of the early to late Archean mantle from Hf-Nd-Ce isotope systematics in basalts and komatiites from the Pilbara Craton21
Rise and fall of the Acadian altiplano: Evidence for a Paleozoic orogenic plateau in New England21
Hf isotopic ratios in zircon reveal processes of anatexis and pluton construction21
Impact of power-law rheology on the viscoelastic relaxation pattern and afterslip distribution following the 2010 Mw 8.8 Maule earthquake21
Bulk composition of regolith fines on lunar crater floors: Initial investigation by LRO/Mini-RF21
Long-term Phanerozoic sea level change from solid Earth processes21
Widespread silicic and alkaline magmatism synchronous with the Deccan Traps flood basalts, India21
Experimental stabilization of carbonate sediments to calcite: Insights into the depositional and diagenetic controls on calcite microcrystal texture21
Island-wide variation in provenance of riverine sedimentary organic carbon: A case study from Taiwan21
Crack to pulse transition and magnitude statistics during earthquake cycles on a self-similar rough fault21
Shale and pyrite Re-Os ages from the Hornby Bay and Amundsen basins provide new chronological markers for Mesoproterozoic stratigraphic successions of northern Canada20
Major Early-Middle Devonian oceanic oxygenation linked to early land plant evolution detected using high-resolution U isotopes of marine limestones20
Deglaciation of Pope Glacier implies widespread early Holocene ice sheet thinning in the Amundsen Sea sector of Antarctica20
Late Ediacaran paleogeography of Avalonia and the Cambrian assembly of West Gondwana20
Role of erosion in creating thrust recesses in a critical-taper wedge: An example from Eastern Tibet20
The coupled Hf-Nd isotope record of the early Earth in the Pilbara Craton20
Local melt contamination and global climate impact: Dating the emplacement of Karoo LIP sills into organic-rich shale20
Miocene to present oceanographic variability in the Scotia Sea and Antarctic ice sheets dynamics: Insight from revised seismic-stratigraphy following IODP Expedition 38220
Partial melting of ultrahigh-pressure eclogite by omphacite-breakdown facilitates exhumation of deeply-subducted crust20
Integrated magnetotelluric and petrological analysis of felsic magma reservoirs: Insights from Ethiopian rift volcanoes20
Fluid overpressure in subduction plate boundary caused by mantle-derived fluids20
A high-resolution map of Hawaiian ULVZ morphology from ScS phases20
High pressure-temperature phase relations of basaltic crust up to mid-mantle conditions20
Phyllosilicate controls on magnesium isotopic fractionation during weathering of granites: Implications for continental weathering and riverine system20
Granite geochemistry is not diagnostic of the role of water in the source20
Covariation of cross-divide differences in denudation rate and χ: Implications for drainage basin reorganization in the Qilian Shan, northeast Tibet20
Ancient refractory asthenosphere revealed by mantle re-melting at the Arctic Mid Atlantic Ridge20
Mountain building, mantle convection, and supercontinents: revisited20
Long-term evolution of terrestrial weathering and its link to Earth's oxygenation20
Reworking subducted sediments in arc magmas and the isotopic diversity of the continental crust: The case of the Ordovician Famatinian crustal section, Argentina20
Breakup with benefits - hydrothermal mineral systems related to the disintegration of a supercontinent20
Toarcian climate and carbon cycle perturbations – its impact on sea-level changes, enhanced mobilization and oxidation of fossil organic matter19
The cascading foreshock sequence of the Ms 6.4 Yangbi earthquake in Yunnan, China19
Meso- to nano-scale evidence of fluid-assisted co-seismic slip along the normal Mt. Morrone Fault, Italy: Implications for earthquake hydrogeochemical precursors19
Controls by rheological structure of the lithosphere on the temporal evolution of continental magmatism: Inferences from the Pannonian Basin system19
Isotopic disequilibrium of Cu in marine ferromanganese crusts: Evidence from ab initio predictions of Cu isotope fractionation on sorption to birnessite19
Constraints on Archean crust recycling and the origin of mantle redox variability from the δ44/40Ca – δ18O – fO2 signatures of cratonic eclogites19
Seismic swarms produced by rapid fluid injection into a low permeability laboratory fault19
Asian monsoon evolution linked to Pacific temperature gradients since the Late Miocene19
“Brittle structural facies” analysis: A diagnostic method to unravel and date multiple slip events of long-lived faults19
Late Triassic uplift, magmatism and extension of the northern North China block: Mantle signatures in the surface19
Onset of magma ocean solidification on Mars inferred from Mn-Cr chronometry19
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